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Loại tài liệu: Tài liệu số - Journal Aticle
Thông tin trách nhiệm: Pavlov, A.V.
Nhà Xuất Bản: Elsevier
Năm Xuất Bản: 1981
Seasonal and annual peculiarities of the soil heat-balance regime in the north of the U.S.S.R. arerndiscussed, and a reduction in the ratio between heat expenditure on evaporation and radiation balance with in creasing latitude is revealed. In contrast, the ratio between heat flow to the soil and radiation balance is shown to increase northwards. Data on the thermal conductivity of soil cover and peat are systematized, and energy exchange processes between the soil and atmosphere are estimated qualitatively by the removal or disturbance of the turf-vegetation layer.rnHeat-balance peculiarities of the forest landscapes of Siberia are compared with open sites, and the limits to changes of balance components by forest removal are identtfied.
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